Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-02T18:54:30.243Z Has data issue: false hasContentIssue false

Host control of recrystallized quartz grains

Published online by Cambridge University Press:  05 July 2018

D. M. Ransom*
Affiliation:
Central Pacific Minerals N.L., Alice Springs, N.T., Australia

Summary

The results of a petrofabric study on recrystallization of quartz in nature are presented and compared with recent experimental work. The orientations of newly recrystallized quartz grains are shown to be dependent on the orientation of host grains from or in which they grew. The results are compatible with the experiments of Hobbs (1968). The orientation of new grains appears to be unrelated to stress.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1971

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Barrett, (C.S.) and Massalski, (T.B.), 1966. Structure of Metals. (McGraw-Hill).Google Scholar
Brace, (W.F.), 1960. Orientation of anistropic minerals in a stress field. Geol. Soc. Amer. Mere. 79, 920.Google Scholar
Griggs, (D.T.), Paterson, (M.S.), Heard, (H.C.), and Turner, (F.J.), 1960. Annealing recrystallization in calcite crystals and aggregates. Ibid. 21-37.CrossRefGoogle Scholar
Horns, (B.E.), 1966. The structural environment of the northern part of the Broken Hill orebody. Journ. Geol. Soc. Aust. 13, 315.38.Google Scholar
Horns, (B.E.), 1968. Recrystallization of single crystals of quartz. Tectonophysics, 6.CrossRefGoogle Scholar
Ransom, (D.M.), Vernon, (R.H.), and Williams, (P.F.), 1968. The Broken Hill orebody, Australia—-a review of recent work. Mineralium Deposita. 3, 293.316.Google Scholar
Kamb, (W.B.), 1959. Theory of preferred crystal orientation by crystallization under stress. Journ. Geol. 67, 153.70.Google Scholar
Kamb, (W.B.), 1961. The thermodynamic theory of non-hydrostatically stressed solids. Journ. Geophys. Res. 66, 259-71.CrossRefGoogle Scholar
Plummer, (H.C.), 1940. Probability and Frequency. London (Macmillan).Google Scholar
Ransom, (D.M.), 1969. Structural and metamorphic studies at Broken Hill. Austr. Nat. Univ. Ph.D. thesis (unpublished).Google Scholar
Sylvester, (A.G.) and Crmlstie, (J.M.), 1968. The origin of crossed girdle orientations of optic axes in deformed quartzites. Journ. Geol. 76, 571.80.Google Scholar
Vernon, (R.H.), 1969. Archaean rocks of the Barrier Ranges. The geology of the Willyama Complex, Broken Hill area. Journ. Gëeol Soc. Austr., N.S. W. Vol (in press).Google Scholar
Vernon, (R.H.), and Ransom, (D.M.), 1970. Retrograde schist-zones of almandine-amphibolite grade. Ibid. (in press).Google Scholar